Passive seismic recording of cryoseisms in Adventdalen, Svalbard

A series of transient seismic events were discovered in passive seismic recordings from 2D geophone arrays deployed at a frost polygon site in Adventdalen, Svalbard. These events contain a high proportion of surface wave energy and produce high-quality dispersion images through an innovative source...

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Main Authors: Romeyn, Rowan, Hanssen, Alfred, Ruud, Bent Ole, Stemland, Helene Meling, Johansen, Tor Arne
Format: Text
Language:English
Published: 2020
Subjects:
Ice
Online Access:https://doi.org/10.5194/tc-2020-141
https://tc.copernicus.org/preprints/tc-2020-141/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd85793 2023-05-15T13:05:36+02:00 Passive seismic recording of cryoseisms in Adventdalen, Svalbard Romeyn, Rowan Hanssen, Alfred Ruud, Bent Ole Stemland, Helene Meling Johansen, Tor Arne 2020-06-25 application/pdf https://doi.org/10.5194/tc-2020-141 https://tc.copernicus.org/preprints/tc-2020-141/ eng eng doi:10.5194/tc-2020-141 https://tc.copernicus.org/preprints/tc-2020-141/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-2020-141 2020-07-20T16:22:04Z A series of transient seismic events were discovered in passive seismic recordings from 2D geophone arrays deployed at a frost polygon site in Adventdalen, Svalbard. These events contain a high proportion of surface wave energy and produce high-quality dispersion images through an innovative source localisation approach, based on apparent offset resorting and inter-trace delay minimisation, followed by cross-correlation beamforming dispersion imaging. The dispersion images are highly analogous to surface wave studies of pavements and display a complex multimodal dispersion pattern. Supported by theoretical modelling based on a highly simplified arrangement of horizontal layers, we infer that a ~ 3.5–4.5 m thick, stiff, high-velocity layer overlies a ~ 30 m thick layer that is significantly softer and slower at our study site. Based on previous studies we link the upper layer with syngenetic ground-ice formed in aeolian sediments, while the underlying layer is linked to epigenetic permafrost in marine-deltaic sediments containing unfrozen saline pore water. Comparing events from spring and autumn shows that temporal variation can be resolved via passive seismic monitoring. The transient seismic events that we record occur during periods of rapidly changing air temperature. This correlation along with the spatial clustering along the elevated river terrace in a known frost polygon, ice-wedge area and the high proportion of surface wave energy constitutes the primary evidence for us to interpret these events as frost quakes, a class of cryoseism. In this study we have proved the concept of passive seismic monitoring of permafrost in Adventdalen, Svalbard. Text Adventdalen Ice permafrost Svalbard wedge* Copernicus Publications: E-Journals Adventdalen ENVELOPE(16.264,16.264,78.181,78.181) Svalbard
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description A series of transient seismic events were discovered in passive seismic recordings from 2D geophone arrays deployed at a frost polygon site in Adventdalen, Svalbard. These events contain a high proportion of surface wave energy and produce high-quality dispersion images through an innovative source localisation approach, based on apparent offset resorting and inter-trace delay minimisation, followed by cross-correlation beamforming dispersion imaging. The dispersion images are highly analogous to surface wave studies of pavements and display a complex multimodal dispersion pattern. Supported by theoretical modelling based on a highly simplified arrangement of horizontal layers, we infer that a ~ 3.5–4.5 m thick, stiff, high-velocity layer overlies a ~ 30 m thick layer that is significantly softer and slower at our study site. Based on previous studies we link the upper layer with syngenetic ground-ice formed in aeolian sediments, while the underlying layer is linked to epigenetic permafrost in marine-deltaic sediments containing unfrozen saline pore water. Comparing events from spring and autumn shows that temporal variation can be resolved via passive seismic monitoring. The transient seismic events that we record occur during periods of rapidly changing air temperature. This correlation along with the spatial clustering along the elevated river terrace in a known frost polygon, ice-wedge area and the high proportion of surface wave energy constitutes the primary evidence for us to interpret these events as frost quakes, a class of cryoseism. In this study we have proved the concept of passive seismic monitoring of permafrost in Adventdalen, Svalbard.
format Text
author Romeyn, Rowan
Hanssen, Alfred
Ruud, Bent Ole
Stemland, Helene Meling
Johansen, Tor Arne
spellingShingle Romeyn, Rowan
Hanssen, Alfred
Ruud, Bent Ole
Stemland, Helene Meling
Johansen, Tor Arne
Passive seismic recording of cryoseisms in Adventdalen, Svalbard
author_facet Romeyn, Rowan
Hanssen, Alfred
Ruud, Bent Ole
Stemland, Helene Meling
Johansen, Tor Arne
author_sort Romeyn, Rowan
title Passive seismic recording of cryoseisms in Adventdalen, Svalbard
title_short Passive seismic recording of cryoseisms in Adventdalen, Svalbard
title_full Passive seismic recording of cryoseisms in Adventdalen, Svalbard
title_fullStr Passive seismic recording of cryoseisms in Adventdalen, Svalbard
title_full_unstemmed Passive seismic recording of cryoseisms in Adventdalen, Svalbard
title_sort passive seismic recording of cryoseisms in adventdalen, svalbard
publishDate 2020
url https://doi.org/10.5194/tc-2020-141
https://tc.copernicus.org/preprints/tc-2020-141/
long_lat ENVELOPE(16.264,16.264,78.181,78.181)
geographic Adventdalen
Svalbard
geographic_facet Adventdalen
Svalbard
genre Adventdalen
Ice
permafrost
Svalbard
wedge*
genre_facet Adventdalen
Ice
permafrost
Svalbard
wedge*
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2020-141
https://tc.copernicus.org/preprints/tc-2020-141/
op_doi https://doi.org/10.5194/tc-2020-141
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